Secondary (s-waves) are transverse waves that travel through the Earth from an earthquake
Primary (p-waves) are longitudinal waves that travel through the Earth from an earthquake
Progressive waves are waves where the peaks and troughs, or compressions and refractions, move through the medium as energy is transferred.
Longitudinal waves are waves that oscillate parallel to the direction of energy transfer.
Transverse waves are waves that oscillate perpendicular to the direction of energy transfer.
Peaks are the maximum positive amplitude of transverse waves
Troughs are the maximum negative amplitudes of a transverse wave
Frequency = 1 / time period measured in Hz
Wave speed = wave length x frequency measured in m/s
Electromagnetic spectrum
radio waves
microwaves
infrared
visible light
ultra violet
x-rays
gamma rays
Speed of light = 3.0 x 10^8 m/s
The frequency is the number of oscillations in one second
Waves transfer energy without transferring matter. You can also use waves to transfer information eg radio waves
Transverse waves eg any electromagnetic wave travel through a vacuum whereas longitudinal waves eg sound waves have to travel through a medium
Earthquake waves
primary waves - cause the initial tremors and are longitudinal waves thaat push or pull on material
secondary waves - slower waves that causetremors a few minutes later and are transverse waves which shake material side to side (cannot travel through liquid)
L waves - they are the slowest wave
Humans have a hearing in the range of roughly 20Hz - 20000Hz anything higher than this is known as ultrasound
Refraction of waves is the change of the direction in which they are travelling when they cross a boundary between one medium and another. This due to the change in speed of the wave in different mediums
Compressions are moving regions in which the medium is denser or has a higher pressure than the surrounding medium
Rarefactions are moving regions in which the medium is less dense or has less pressure then the surrounding medium
Equilibrium position is the resting position of waves or particles in an oscillation
Resorting force is a force that tries to return a system to its equilibrium position
The direction of a particle in a wave is shown by the rule that the particle is going towards the postion of the particles behind it
Phase difference = distance between particle (x) / wave length (λ) x 360
Wavelength is the minimum distance between two point in phase on adjacent waves
Displacement is the distance from the equalibrium position in a particluar direction
Amplitude is the maximum displacement from the equalibrium position of a wave.
Reflection vs Refraction
frequency doesn’t change in both
both happen with all waves
refraction in waves changes from one medium to another whereas reflection is in one medium
wave speed is directly proportional to the wave length eg is wave speed decreases so does the wave length
all angles are measured from the normal
ray bends towards the normal then the wave is slowing down
ray bends away from the normal then the wave has sped up
refractive index of a material (n) = speed of light in a vacuum (C) / speed of light through the material (V)
The angle at which the light is bent depends in the relative speeds of light through the two materials
The greater the refractive index the move the light entering the material is refracted towards the normal